Soil Hydraulic Conductivity and Soil Water Retention of Inland Peat on Various Land Covers (Case Study: Natural Peat and Burnt Peat)

Q3 Agricultural and Biological Sciences
F. F. Adji, N. Yulianti, Z. Damanik, Bina Candra, Akhmat Sajarwan, S. Winerungan, U. Darung, Mofit Saptono, Rony Teguh, S. Grover, Gita Josefhine Sitohang, Melda Reskiony Sitorus
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引用次数: 0

Abstract

: This research aims to examine differences in the rate of saturated soil hydraulic conductivity (permeability) and unsaturated soil hydraulic conductivity (infiltration) and soil water retention with various pressures in peatland with different land covers. The study was conducted from June to October 2021. The research was conducted at the LAHG-Sebangau and at the KHDTK-Tumbang Nusa, central Kalimantan, Indonesia. Based on the results of this study, at the HA site has the highest saturated soil hydraulic conductivity (permeability) rate at a depth of 0-10 cm was classified as rather fast. The lowest saturated soil hydraulic conductivity (permeability) rate of the HS site at a depth of 20-30 cm was classified as a rather slow. The highest unsaturated soil hydraulic conductivity (infiltration) rate was at the HS site at a depth of 0-10 cm was classified as fast, while the lowest was at the natural forest (HA) at a depth of 10-20 cm classified as very slow. The soil physical characteristics: Soil water content ranging from 474.769-631.364%, fiber content ranging from 8.00-22.67%, bulk density ranging from 0.12-0.19 g cm -3 , porosity ranging from 71.61-85.63% and the color of the soil is dark brown to very blackish red dark. Meanwhile, the ability of the soil to accommodate maximum soil water (saturated conditions) with the highest pF 0 is at the HK site at depth of 10-20 cm was 377,92 cm 3 cm -3 , while the lowest is in the HR site at depth of 0-0 cm is 31.11 cm 3 cm -3 . The ability of the soil in maximum soil water holding (water control conditions) at pF 4.2 is highest in the HS site at depth of 20-30 cm was 61.10 cm 3 cm -3 , while the lowest is in the HR site at depth of 0-10 cm was 13.30 cm 3 cm -3 . The soil porosity value in the HS site was higher than that of the HR site, which is 85,830 and 82,130%. The weight value of particle at the HS site was higher compared to other land cover ranging from 0.74-0.86 g cm -3 . The weight value of bulk density at the HS site ranging from 0.17-0.19 g cm -3 was higher than other land cover.
不同土地覆被条件下内陆泥炭的土壤导电性与土壤保水性(以天然泥炭和烧泥炭为例)
本研究旨在研究不同土地覆盖条件下泥炭地饱和土导水率(渗透率)和非饱和土导水率(入渗率)和土壤保水率在不同压力下的差异。该研究于2021年6月至10月进行。该研究在印度尼西亚加里曼丹中部的LAHG-Sebangau和KHDTK-Tumbang Nusa进行。基于本研究的结果,在HA位点饱和土壤的水力导水率(渗透率)最高,深度为0-10 cm,被归类为较快。在20 ~ 30 cm深度,HS站点的饱和土导流率(渗透率)最低,属于较慢。非饱和土壤渗透速率最高的是HS样地,深度为0 ~ 10 cm,为快速;最低的是天然林样地,深度为10 ~ 20 cm,为极慢。土壤物理特征:土壤含水量为474.769-631.364%,纤维含量为8.00-22.67%,容重为0.12-0.19 g cm -3,孔隙度为71.61-85.63%,土壤颜色为深褐色至极黑红色。同时,在10 ~ 20 cm的HK站点,土壤对最大土壤水分(饱和条件)的容水能力最高,为377,92 cm 3 cm -3,而在0 ~ 0 cm的HR站点,土壤容水能力最低,为31.11 cm 3 cm -3。土壤在pF 4.2条件下的最大持水能力(控水条件)在20 ~ 30 cm的土壤中最高,为61.10 cm 3 cm -3,而在0 ~ 10 cm的土壤中最低,为13.30 cm 3 cm -3。高通量土壤孔隙度值高于高通量土壤孔隙度值,分别为85,830%和82,130%。HS站点的颗粒重量值高于其他土地覆盖,在0.74 ~ 0.86 g cm -3之间。HS样地容重权重值在0.17 ~ 0.19 g cm -3之间,高于其他样地。
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来源期刊
OnLine Journal of Biological Sciences
OnLine Journal of Biological Sciences Agricultural and Biological Sciences-Agricultural and Biological Sciences (all)
CiteScore
2.10
自引率
0.00%
发文量
35
期刊介绍: :: Cell biology :: Developmental biology :: Structural biology :: Microbiology :: Molecular biology & genetics :: Biochemistry :: Biotechnology :: Biodiversity :: Ecology :: Marine biology :: Plant biology :: Bioinformatics
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